T.W. Dibblee Jr.
1972, Open-File Report 72-91
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Page 5625, results 140601 - 140625
Publication Extents
Not all publications have extents, not all extents are completely accurateL.A. Wagner, P.H. Hamecher
1972, Open-File Report 72-437
In June 1972, tropical storm Agnes caused sever flooding in Pennsylvania and southern New York. The flood, on many major streams were the highest known since the river valleys were settled. Maximum discharges were as much as twice the discharge of a 50-year flood. In southern New York, large areas...
L.A. Swallow, W.J. Schneider
1972, Open-File Report 72-370
No abstract available....
L.A. Wagner, P.H. Hamecher
1972, Open-File Report 72-434
In June 1972, tropical storm Agnes caused sever flooding in Pennsylvania and southern New York. The flood, on many major streams were the highest known since the river valleys were settled. Maximum discharges were as much as twice the discharge of a 50-year flood. In southern New York, large areas...
G. E. Hendrickson, C. J. Doonan
1972, Hydrologic Atlas 426
W. H. Langer
1972, IMAP 784-G
W. H. Langer
1972, IMAP 784-F
J. C. Reed Jr., J. R. Keith
1972, IMAP 786-B
D.E. Wilhelms
1972, IMAP 722
The distribution of major physiographic provinces and geologic units of the Tarantius quadrangle is determined by the five intersecting circular multi-ringed mare basins. Three basins, i<span...
G.M. Richmond, H.A. Waldrop
1972, IMAP 638
H. A. Pohn
1972, IMAP 713
The Tycho quadrangle is centrally located in the southern half of the earthside hemisphere of the Moon. The area is characterized by a high density of craters, the largest of which <span...
Paul L. Williams
1972, IMAP 591-L
The term “landslide” is broadly defined as any “downward and outward movement of slope-forming materials composed of natural rock, soils, artificial fills, or combinations of these materials. The moving mass may proceed by any one of three principal types of movement: falling, sliding, or flossing, or by their combinations” (Varnes,...
D.F. Goerlitz, Eugene Brown
1972, Techniques of Water-Resources Investigations 05-A3
L.A. Weiss
1972, IMAP 784-Q
Paul L. Williams
1972, IMAP 591-J
This map shows the relative ease (or difficulty) with which rocks and surficial deposits can be excavated. Because of rapidly changing technology of excavation and considerable local variability of many rock units, it is not practical to specifically categorize rock units according to type of equipment needed for their excavations....
D.E. Stuart-Alexander, E.M. Shoemaker, H. J. Moore
1972, IMAP 674
Paul L. Williams
1972, IMAP 591-H
No abstract available....
J. D. Love, H. F. Albee
1972, IMAP 769-A
K.M. Waddell, Don Price
1972, Hydrologic Atlas 417
The United States Geological Survey, in cooperation with the Utah Department of Natural Resources, Division of Water Rights, began a reconnaissance in 1967 to obtain essential water-quality information for the Bear River basin. The reconnaissance was directed toward defining the chemical quality of the basin’s surface waters, including suitability for...
G.L. Richmond, K. L. Pierce, H.A. Waldrop
1972, IMAP 710
J. O. Maberry
1972, IMAP 770-G
No abstract available....
I. J. Witkind
1972, IMAP 781-C
No abstract available....
J. O. Maberry
1972, IMAP 770-C
J. O. Maberry
1972, IMAP 770-F
No abstract available....
Glenn R. Scott
1972, IMAP 790-C
Formations that contain clays having swelling pressures higher than 2,500 pounds per square foot (as measured by the Potential Volume Change meter) are listed in order of decreasing swelling pressure: Denver Formation, Pierre Shale, Laramie Formation, Green Mountain Conglomerate, Fox Hills Sandstone, and Arapahoe Formation. Some landslides derived from these...